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大洋钻探与冲绳海槽
引用本文:李乃胜.大洋钻探与冲绳海槽[J].地球科学进展,1995,10(3):240-245.
作者姓名:李乃胜
作者单位:中国科学院海洋研究所
摘    要:在多次赴冲绳海槽地球物理调查的基础上,综合国内外的调查研究成果,对冲绳海槽地质构造学研究的历史、已查明了地球物理场特征,海底构造特征和需要进一步探讨了问题作了系统的总结,阐明了ODP在冲绳海槽钻探的重要意义。

关 键 词:大洋钻探  冲绳海槽  地质构造

ODP AND THE OKINAWA TROUGH
Li Naisheng.ODP AND THE OKINAWA TROUGH[J].Advance in Earth Sciences,1995,10(3):240-245.
Authors:Li Naisheng
Institution:Institute of Oceanology,The Chinese Academy of Sciences,Qingdao  266071
Abstract:The Okinawa Trough which develops at the east part of the East China sea is a active rifting basin and has a series of typical geological and geophysical features as a active modern rifting valley,such as well-developed rift graben,very high heat-flow values and abundant thermal fluid activity,strong crust extension,frequent volcanic and earthquake activity,and a lot of submarine extensional faults. But up to now,there have been many scientific problems which need deep drilling data to be finally solved .ODP's drilling in the Okinawa Trough is of great scientific significance for China.
Keywords:Okinawa Trough  ODP  Geological structure  
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